Dodge City times. [volume] (Dodge City, Kan.) 1876-1892, 1887-11-24
CONCERNING OUDS.


: Their Nature, Form+, TompOs. ton, ve-
locity. Height, Etc.
a cloud is mass Of visible vapcr OF
water particles held in suspension in
the atmosphere. If it rests upon tho
surface of the earth we call it fog:
We sec mass of vapor on the sum.
NIT Of a high mountain and we cal
it cloud. but if we climb to the top OF
the mountain and find ourselves in the
cloud We see it to be simply fog. TIC
our observation. clouds take on forms
that are almost infinite in variety.
yet they may be divided into six
classes. each presenting quite distinct
characteristics. These are known as
cirrus. cumulus and stratus cloud. rs
simple divisions; and GIRO cumulus.
cirro-stratus and cumulO-stratus rs
compound divisions. The cirrus
cloud consists of long. slender. fila
ments. either parallel or diverging
from each other. These clouds have
the greatest elevation and the least
density of all clouds. Even in fail
weather the sky is seldom free from
small distant groups of irrus clouds.
They are thought 10 be mad C up OF
spicule of ice or flakes of snow. since
at the great height at which
they float, from five to eight miles
above the earth. the temperature of
the air is below freezing point even in
midsummer The cumulus cloud is
much denser than the cirrus and is
formed nearer the earth. 1t usually
has the form of hemispherical or
convex mass with horizontal base.
This is the cloud often seen in large
masses near the horizon. looking like
huge mountains of snow. The round
ed top of this cloud results from the
mode of its formation. AS the earth
is heated by the suns rays. currents
of warm air rise. carrying with them
invisible vapor. When they reach a
certain height this vapor is condensed
! and forms cloud. and since the upward
motion is greater under the center Of
the cloud. the vapor is then carried to
its greatest height. The stratus cloud
is widely-extended, horizontal sheet.
often covering the entire Sky, and
and hanging SO low that it frequently
touches the earth's surface in the
form of q fog. For the compound
notifications of cloud forms. the cir
, ro-cu nulus is seen in small rounded
mass, S. often very near together On
account of their fleecy appearance
these are often called 'woolly clouds. y
This cloud is very frequent in summer.
! but seldom precedcs rain. The GIRO
stratus consists OF tibrous clouds
spread out in strata, which are
F., either horizontal or slightly in
clincd 10 the horizon. Sometimes the
whole sky is notified with the cloud.
| looking like the back of n mackcrel.
/ and, therefore, il called 4 mackcrel
sky. This cloud always presages wind
and rain. The cumulo-stratus is the
large dark cloud formed by the mass.
ing of the tlcecy cumulus in great
heaps. These clouds are to be seen in
great magnificencc on the approach of
thunderstorm, and are. therefore.
often called thunder heads Some
! metcoroIogists also classify with the
above the nimbus cloud, which is Il
stratus cloud from which rain is fall
ing but others do not think it worth
while to keep this division. The
height of a cloud is measured by
trigonometrical rule by observing its
direction simultaneously ut two sta
tons. In mountainous countries it
can be compared with the peaks near
{ which it passes. Most accurate re-
suits, however, arc obtained by ascend
ing in balloon and no ing the hei ght
of the barometer when entering the
cloud and again when emerging from
it, the barometer giving the means of
computing corresponding attitudes.
The height of clouds is very variable
The stratus, as we have said, often
descending to the earth. II pleasant
weather tho lower limit of cumulus
clouds varies from 3 JO) to 1000 feet
elevation. and Their upper limit from
5. GO to - 90 0 feet. Cirrus Clouds never
descend te.ow tho summit of Mount
B.anc. which has a height of Is,
feet, and are often seen to be far above
mountains that are 10000 to $4,000
feet high. 1t is estimated. however,
that they would not be visible at a
height exceeding ten miles. In verti-
cal thickness clouds arc supposed to
seldom exceed half mile, but the
enormous masses Of cumul..s are
sometimes estimated at over three
miles. Clouds move with the wind.
and there is no way of estimating their
movement but by measuring the
velocity of the wind currents. Clouds
reflect light. of course, or they would
not be visible; such light as can pass
path by the presence of the vapor
particles. Thus. when we see objects
through fog we often notice that
they are distant from their true posi-
ton or nnnaturally magnified. The
effect of clouds on heat is 10 lessen it,
the water particles absorbing it, and
lowering the temperature of the air by
their conversion into invisible vapor.
Nevertheless. cloud, hanging low in
cold weather prevent fall If tenn
peraturc by preventing the radiation
of heat from the earth's surface. As
to moisture. clouds arc, obviously.
moisture itself rs well as its cause
Chicago lpter-Ocean.
WILTER'S WEAKNESS.